Selective adsorption of L- and D-amino acids on calcite: Implications for biochemical homochirality

Proc Natl Acad Sci U S A. 2001 May 8;98(10):5487-90. doi: 10.1073/pnas.101085998. Epub 2001 May 1.

Abstract

The emergence of biochemical homochirality was a key step in the origin of life, yet prebiotic mechanisms for chiral separation are not well constrained. Here we demonstrate a geochemically plausible scenario for chiral separation of amino acids by adsorption on mineral surfaces. Crystals of the common rock-forming mineral calcite (CaCO(3)), when immersed in a racemic aspartic acid solution, display significant adsorption and chiral selectivity of d- and l-enantiomers on pairs of mirror-related crystal-growth surfaces. This selective adsorption is greater on crystals with terraced surface textures, which indicates that d- and l-aspartic acid concentrate along step-like linear growth features. Thus, selective adsorption of linear arrays of d- and l-amino acids on calcite, with subsequent condensation polymerization, represents a plausible geochemical mechanism for the production of homochiral polypeptides on the prebiotic Earth.

Publication types

  • Research Support, Non-U.S. Gov't

MeSH terms

  • Adsorption
  • Amino Acids / metabolism*
  • Calcium Carbonate / metabolism*
  • Stereoisomerism

Substances

  • Amino Acids
  • Calcium Carbonate